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r <br /> 23 May 2003 <br /> AGE-NC Project No 95-0184 <br />' Page 7 of 9 <br /> prevalent and coarser (gravelly sand Identified at 95 feet) with depth Based on <br />' CPT-generated lithologic properties, AGE Identified a vadose zone extending from surface <br /> grade to approximately 35 feet bsg and fourteen hydrologic units Five hydrologic units <br />' (HU5, HU7 and HU9, HU11 and HU13) are sand-bearing units of low dynamic pore <br /> pressures,the remaining units are predominantly zones of inter-bedded clayey silt,silty clay, <br /> clay and stiff fine-grained sediment, with occasional, laterally discontinuous sand lenses, <br />' pore pressures within these intervals vary from low to high <br /> • The most recent ground water monitoring data place depth to ground water at approximately <br /> 35 feet bsg, however, historical ground water data compiled by the San Joaquin County <br />' Flood Control and Water Conservation District between 1970 and 2003 indicated that ground <br /> water at the site has been as deep as 70 to 75 feet bsg The dominant ground water flow <br />' direction is generally northward across much of the site,however,in the southeastern portion <br /> of the site the inferred ground water flow direction is generally easterly 4bi.,S e -r`.' <br /> • On 24 April 1987, one 1,000-gallon gasoline underground storage tank (Tank A) was _ I <br />' remo d from the northwestern corner of the site,on 19 October 1988,one 300-gallon waste <br /> oil UST(T B)was removed from the site near the northern property line and the canopy, <br /> 4\ , and on 25 May 1990, one 1,000-gallon gasoline UST and one 1,000-gallon diesel UST <br />' (Tanks C & D) were removed from beneath the sidewalk at the southeastern corner of the <br /> 12, site Petroleum hydrocarbons were detected in soil samples collected beneath tanks A,C and <br /> D, only low concentrations of TCE and chloroform were detected in the sample collected <br />' beneath Tank B <br /> • The timings of the releases from the USTs are unknown, however, once released to the <br />' subsurface, the contaminants migrated vertically and laterally The deep vertical extent of <br /> contaminated soil and ground water at the site suggests that the releases occurred when <br /> ground water elevation was low, either during a drought penod(s) and/or a period of heavy <br />' ground water withdrawal <br /> • The cores of highest contaminated soil appear to be from between 35 and 45 feet bsg at the <br />' northern tank location and at approximately 25 feet bsg at the southern tanks location, <br /> however, the lateral and vertical extent of contaminated soil has not been defined at either - G <br /> locations <br /> • Petroleum hydrocarbon compounds and VOCs have been detected in ground water to the <br /> total depth of the CPT borings (approximately 180 feet bsg), the highest,concentrations of <br />' contaminants in water samples collected from the CPT borings were generally from <br /> hydrologic units in fine-grained soil Laterally,the extent of ground water contamination has <br /> not been defined <br /> I <br /> IAdvanced GeoEnviron mental,Inc <br /> I <br />